Cui Zhijiu, Wu Yongqiu, Liu Gengnian, Ge Daokai, Xu Qinghai,Pang Qiqing, Yin Jiarun. 1998. Records of natural exposures on the Kunlun Shan Pass of Qinghai Xizang Highrood. In: Shi Yafeng, Li Jijun, Li Bingyuan, ed. Uplift and Environmental Changes of Qinghai- Xizang (Tibetan) Plateau in the Late Cenozoic. Guangzhou: Guangdong Science and Technology Press, 81～114 (in Chinese ).
[10]
Li Bingyuan. 2000. Greatest lake period on the Tibetan Plateau . Acta Geographica Sinica, 55(2) : 174～181(in Chinese with English abstract).
[11]
Liu Lansuo. 1982. The Pliocene- early Pleistocene spore-pollen assemblage along the Qinghai- Xizang highway and its significance. Contributions to the Geology of the QinghaiXizang (Tibet)Plateau (4). Beijing: Geol. Pub. House, 136～50 (in Chinese ).
[12]
Lu Houyuan, Wang Shuyun, Shen Caiming, et al. 2004. Spatial pattern of modern Abies and Picea pollen in the Qinghai-Xizang Plateau. Quaternary Sciences, 1:39～49 (in Chinese with English abstract).
[13]
Lynch E A. 1996. The ability of pollen from small lakes and ponds to sense fine-scale vagetation patterns in the Central Rocky Mountains, USA. Review of palaeobotany and Palynology, 94:197～210.
[14]
Qian Fang, Zhang Jingqi. 1996. Discovery of the Hipparion sp. at the Kunlun pass of Golmud and quantitative study on neotectonism.Journal of Geomechanics, 2(English supplement):139～147.
[15]
Shi Yafeng, Yu Ge, Liu Xiaodong, Li Bingyuan, Yao Tandong.2001. Reconstruction of the 30～40 ka BP enhanced Indian monsoon climate based on geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology,169: 69～83(in Chinese with English abstract).
[16]
Spear R W. 1989. Late- Quatenary history of hight elevation vegetation in the White Mountains of New Hampshire.Ecologycal Monographs, 59:125～151.
[17]
Wu Yushu, Xiao Jiayi. 1995. A preliminary study on modern pollen rain of Zabuye salt lake area, Xizang. Acta Botanica Yunnan, 17(1) :72～78(in Chinese with English abstract).
[18]
Yao Tandong, Thompson L G, Shi Yafeng, Qin Dahe, Jiao Keqin,Yang Zhihong, Tian Lide, E. Mosley-Thompson. 1997.Climate variation since the last interglaciation recorded in the Guliya ice core. Science in China(series D), 27(5) :447～452(in Chinese).
[19]
Zheng Mianping, Meng Yifen, Wei Lejun. 2000. Evidence of the Pan-Lake Stage in the Period of 40～28 ka BP on the QinghaiTibet Plateau. Acta Geological Sinica, 74(1): 266～272.
Chen Kezao, Bowler J M, Kelts K. 1990. Palaeoclimatic evolution with in the Qinghai-Xizang(Tibet) Plateau in the last 40 000Years. Quaternary Sciences, (1): 21～30 (in Chinese with English abstract).
[27]
Jackson S T, Smith S J. 1994. Pollen dispersal and representation on an isolanted, forested plateau. New Phitologist, 128:181～193.
[28]
Liu Qisheng, Ye Peisheng, Zhao Xitao, Ma Zhibang. 2003. Discovery of lacustrine deposits in Bu Qu Basin of Changjiang River source and their U-Scries dating. Quaternary Sciences, 23 (1): 111 (in Chinese).
[29]
Luo S D, Ku T L. 1991. U-series isochron dating: A generalized method employing total-sample dissolution. Geochimica et Cosmochimica Acta, 55: 555～564.
[30]
Minckley T, Whitlock C. 2000. Spatial variation of modern pollen in Oregon and southern Washington, USA. Review of Palaeobotany and Palynology, 112: 97～123.
[31]
Qian Fang, Ma Xinghua, Wu Xihao, Pu Qingyu. 1982. Study on the magnetic strata from the Qiangtang and Quguo Formations.Contributions to the Geology of the Qinghai-Xizang (Tibet)Plateau (4). Beijing: Geol. Pub. House, l12～147(inChinese)
[32]
Shan Fashou, Du Naqiu, Kong Zhaochen. 1993. Vagetational and enviroumental changes in the last 350 ka in Erlangzian, Qinhai Lake. Journal of Lake Sienees, 5 (1): 9～17 (in Chinese with English abstract).
[33]
Shi Yafeng, Liu Xiaodong, Li Bingyuan, Yao Tandong. 1999. The correlationship between the event of most strong summer monsoon and precession cycle on the Qinghai Tibetan Plateau during 40～30 ka BP. Chinese Bulletin, 44(14): 1475～1480(in Chinese with English abstract).
[34]
Shi Yafeng, Jia Yulian,Yu Ge,Yang Dayuan, Fan Yunqi, Li Shijie,Wang Yunfei. 2002. Features, impacts and causes of the high temperature and large precipitation event in the Tibetan Plateau and its adjacent area during 40～30 ka BP. Journal of Lake Sciences, 14(1): 1～11(in Chinese).
[35]
Sun Xiangjun, Li Xu. 1999. A pollen record of the last 37 ka in deep sea core 17940 from the nothern slope of the South China Sea.Marine Geology, 156:227～244.
[36]
Weng Chengyu, Sun Xiangjun, Chen Yinshuo. 1993. Numerical haractristics of pollen assemblages of surface samples from the west Kunlun Mountains. Acta Botanica Sinica, 35 (1): 69～79(in Chinese with English abstract).
[37]
Zhao Xitao, Zhu Dagang, Yan Fuhua, Wu Zhonghai, Ma Zhibang,Mai Xueshun. 2003. Climatic change and lake-level variation of Nam Co, Xizang since the last interglacial stage. Quaternary Sciences, 23(1): 41～52(in Chinese with English abstract).
